The origin of along-shelf pressure gradient in the Middle Atlantic Bight Cape Hatteras. It is also shown that the large-scale wind cannot directly affect the aspg. However, north of the Gulf Stream, there exist seasonal and inter-annual variations of eddy kinetic energy which affect the aspg 134.95 Kb. 2
The origin of along-shelf pressure gradient in the Middle Atlantic Bight Cape Hatteras. It is shown that the large-scale wind pattern cannot directly affect the aspg. On the other hand, north of the Gulf Stream, there exist seasonal and inter-annual variations of eddy kinetic energy which affect the aspg 74.87 Kb. 1
Fifth section This judgment will become final in the circumstances set out in Article 44 ยง 2 of the Convention. It may be subject to editorial revision 120.18 Kb. 3